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Grieskogel Mountains

Grieskogelgruppe

Mon 8 Dec

Day Risk Profile

Moderate
below 2000m
Considerable
above 2000m

Avalanche Problems

Above 2000 m

Considerable (3) Dry avalanches · all day
Dry snow level 3 Persistent weak layers Slab 3
N, NE, E, W, NW
above 2000m
Medium Some Very poor
GM.1 GM.3
Field notes

Persistent Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary are very challenging to recognise. Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds and shooting cracks are typical when present, but you can have a serious weak layer with no warning signs at the surface. Knowledge of how the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has evolved is essential. SLF's travel advice is direct: travel conservatively, avoid terrain where the consequences of being caught are large, and treat the history of weather and snow as more important than what you can see today. Read the full bulletin.

Source: SLF Avalanche Bulletin Interpretation Guide

Below 2500 m

Considerable (3) Wet avalanches · all day
Wet snow level 3 Gliding snow Loose 3
All aspects
below 2500m
Small Some Very poor
GM.1 GM.3
Field notes

Almost impossible to predict precisely, even when the warning signs are visible. A crack visible on the snowpack surface formed by snow-gliding on steep, and particularly grass-covered slopes. Areas below slopes with visible glide cracks should be avoided whenever possible due to threat of gliding sluffs or avalanches.EAWS glossary — gaps that open in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary down to the ground — are often precursors to release, but they don't tell you when. A glide avalanche can release minutes after the cracks appear, or weeks later, or not at all. Some release without any visible warning. Avoid lingering anywhere near glide cracks: above them, alongside them, or below in the runout.

Source: SLF Avalanche Bulletin Interpretation Guide

Avalanche Activity

As a consequence of new snow and warming a sometimes unfavourable avalanche situation will prevail. Weakly bonded old snow represents the main danger.

During the first half of the night as the snowfall level rises there will be an appreciable increase in the avalanche danger to level 3 (considerable). Individual natural avalanches are possible during the course of the night, in particular medium-sized ones. Single winter sport participants can release avalanches easily. This applies in particular on steep west, north and east facing slopes above approximately 2000 m. As a consequence of the rain more frequent gliding avalanches and snow slides are possible, but they will be mostly small.

Outlook

Constant avalanche danger

9 December 2025

Gradual decrease in avalanche danger. Weakly bonded old snow represents the main danger.

Snowpack & Weather

Snowpack
Up to 2500 m rain will fall until late morning in some regions. The Snow deposited on the ground in a multiplicity of layers.EAWS glossary will become weakly bonded over a wide area. Faceted Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary exist in the bottom section of the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. This applies especially on west, north and east facing slopes at elevated altitudes, in particular in shady places that are protected from the wind. The fresh and older wind slabs are lying on Transparent, frequently flat crystals forming on the snowpack when moist air settles on the surface. It forms most often during cold, clear, humid nights. Once it is blanketed by fresh fallen snow, surface hoar is one of the most critical weak layer. See also: www.snowcrystals.itEAWS glossary in some places on shady slopes.

Source

ALBINA

Issued

7 Dec 16:00 UTC

Valid until

8 Dec 16:00 UTC

Next update

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